Diamond Exploration Potential of the Northern East European Platform

In this study, we assess the diamond exploration potential of the northern East European Platform based on aeromagnetic survey results and the morphologic and geochemical analysis of 1513 grains of kimberlite indicator minerals (KIMs), such as purple pyrope garnet, olivine, and Cr-diopside. These mi...

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Published in:Minerals
Main Authors: Elena V. Shchukina, Vladimir S. Shchukin
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Online Access:https://doi.org/10.3390/min8050189
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spelling ftmdpi:oai:mdpi.com:/2075-163X/8/5/189/ 2023-08-20T04:05:06+02:00 Diamond Exploration Potential of the Northern East European Platform Elena V. Shchukina Vladimir S. Shchukin agris 2018-05-01 application/pdf https://doi.org/10.3390/min8050189 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/min8050189 https://creativecommons.org/licenses/by/4.0/ Minerals; Volume 8; Issue 5; Pages: 189 diamond exploration kimberlite indicator mineral geochemistry morphology East European Platform Arkhangelsk region Text 2018 ftmdpi https://doi.org/10.3390/min8050189 2023-07-31T21:30:01Z In this study, we assess the diamond exploration potential of the northern East European Platform based on aeromagnetic survey results and the morphologic and geochemical analysis of 1513 grains of kimberlite indicator minerals (KIMs), such as purple pyrope garnet, olivine, and Cr-diopside. These minerals were recovered from samples collected from modern river and stream sediments in four areas located in the north-eastern (within the Arkhangelsk Diamondiferous Province) and south-western (hundreds of kilometers outside of the Arkhangelsk Diamondiferous Province) parts of the Arkhangelsk region in the European part of Russia. All the studied areas are located within ancient cratons, including the Kola, Karelian, and Shenkursk cratons. Based on the major element compositions of the KIMs and thermobarometric calculations, this study confirms that the lithospheric mantle beneath the studied areas is suitable for the formation and preservation of diamonds. The high percentage of KIMs with primary magmatic grain surface morphologies is evidence of the presence of local kimberlite sources within all of the studied areas. The significant amount of diamond-associated KIMs indicates that the potential sources are diamondiferous. Hence, the results suggest that the studied areas can be recommended for further diamond prospecting activity with a high probability of discovering new diamondiferous kimberlites. Text Arkhangelsk karelia* karelian MDPI Open Access Publishing Minerals 8 5 189
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic diamond
exploration
kimberlite indicator mineral
geochemistry
morphology
East European Platform
Arkhangelsk region
spellingShingle diamond
exploration
kimberlite indicator mineral
geochemistry
morphology
East European Platform
Arkhangelsk region
Elena V. Shchukina
Vladimir S. Shchukin
Diamond Exploration Potential of the Northern East European Platform
topic_facet diamond
exploration
kimberlite indicator mineral
geochemistry
morphology
East European Platform
Arkhangelsk region
description In this study, we assess the diamond exploration potential of the northern East European Platform based on aeromagnetic survey results and the morphologic and geochemical analysis of 1513 grains of kimberlite indicator minerals (KIMs), such as purple pyrope garnet, olivine, and Cr-diopside. These minerals were recovered from samples collected from modern river and stream sediments in four areas located in the north-eastern (within the Arkhangelsk Diamondiferous Province) and south-western (hundreds of kilometers outside of the Arkhangelsk Diamondiferous Province) parts of the Arkhangelsk region in the European part of Russia. All the studied areas are located within ancient cratons, including the Kola, Karelian, and Shenkursk cratons. Based on the major element compositions of the KIMs and thermobarometric calculations, this study confirms that the lithospheric mantle beneath the studied areas is suitable for the formation and preservation of diamonds. The high percentage of KIMs with primary magmatic grain surface morphologies is evidence of the presence of local kimberlite sources within all of the studied areas. The significant amount of diamond-associated KIMs indicates that the potential sources are diamondiferous. Hence, the results suggest that the studied areas can be recommended for further diamond prospecting activity with a high probability of discovering new diamondiferous kimberlites.
format Text
author Elena V. Shchukina
Vladimir S. Shchukin
author_facet Elena V. Shchukina
Vladimir S. Shchukin
author_sort Elena V. Shchukina
title Diamond Exploration Potential of the Northern East European Platform
title_short Diamond Exploration Potential of the Northern East European Platform
title_full Diamond Exploration Potential of the Northern East European Platform
title_fullStr Diamond Exploration Potential of the Northern East European Platform
title_full_unstemmed Diamond Exploration Potential of the Northern East European Platform
title_sort diamond exploration potential of the northern east european platform
publisher Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/min8050189
op_coverage agris
genre Arkhangelsk
karelia*
karelian
genre_facet Arkhangelsk
karelia*
karelian
op_source Minerals; Volume 8; Issue 5; Pages: 189
op_relation https://dx.doi.org/10.3390/min8050189
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/min8050189
container_title Minerals
container_volume 8
container_issue 5
container_start_page 189
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